Three Fingered Jack
Three Fingered Jack is a summit of a shield volcano of the Cascade Range in the U.S. state of Oregon. Formed during the Pleistocene epoch, the mountain consists mainly of basaltic andesite lava and was heavily glaciated in the past. While other Oregon volcanoes that were heavily glaciated—such as Mount Washington and Mount Thielsen—display eroded volcanic necks, Three Fingered Jack's present summit is a comparatively narrow ridge of loose tephra supported by a dike only 10 feet (3.0 m) thick on a generally north–south axis. Glaciation exposed radiating dikes and plugs that support this summit. The volcano has long been inactive and is highly eroded.
| Three Fingered Jack | |
|---|---|
Southwest side of Three Fingered Jack seen from Pacific Crest Trail | |
| Highest point | |
| Elevation | 7,844 ft (2,391 m) NAVD 88 |
| Prominence | 756 m (2,480 ft) |
| Coordinates | 44°28′44″N 121°50′35″W |
| Geography | |
| Parent range | Cascades |
| Topo map | USGS Three Fingered Jack |
| Geology | |
| Age of rock | older than 200,000 years |
| Mountain type | Summit, Shield volcano |
| Volcanic arc | Cascade Volcanic Arc |
| Last eruption | Pleistocene |
| Climbing | |
| First ascent | 1923 by E. McNeal and party |
Three Fingered Jack has diverse flora, fauna, and fungi. The Molala people, one of the indigenous groups in the northwestern United States, historically inhabited the area around the volcano. Not much is known about Molala culture, other than that the group fished for salmon and collected berries, fruits, obsidian, and dried herbs. David Douglas was the first person of non-indigenous descent to reach the area in 1825, followed by Peter Skene Ogden the following year. The first group to ascend the volcano reached its summit in September 1923. Three Fingered Jack can still be climbed, but climbers can require rescue after becoming disoriented in low visibility conditions.